TheAppalachian Highlands is one of eightgovernment-defined physiographic divisions of thecontiguous United States.[1] It links with theAppalachian Uplands in Canada to make up theAppalachian Mountains. The Highlands includes seven physiographic provinces, which is the second level in the physiographic classification system in the United States. At the next level of physiographic classification, called section/subsection, there are 20 unique land areas with one of the provinces having no sections.[a]
The Appalachian Highlands are characterized by a diverse physiographic division.[2][3][4]
The seven provinces are:
TheAdirondack Mountains are a circular dome of mountains in Northeastern New York about 160 miles wide with more than 100 peaks, at least 40 that are over 4,000 feet tall. There are over 200 named lakes, with the number of smaller lakes, ponds, and other bodies of water reaching over 3,000. The region has over 1,200 miles of river.[5] The current relief owes much to glaciation. Among the named lakes around the mountains, areLake George,Lake Placid, andLake Tear of the Clouds, which is the source of theHudson River.
TheAdirondack High Peaks are a list of 46 mountains in the Adirondacks that are above or close to 4,000 feet in elevation. The list was created when it was believed that all 46 peaks were at least 4,000 feet tall. Later surveys showed that four of the peaks are actually lower than 4,000 feet. One 4,000 foot peak was also not included in the original list. The tallest peak isMount Marcy, which is the highest point in New York at 5,344 feet (1,629 m). Although the mountains are formed from ancient rocks more than one billion years old, geologically, the 160-mile wide dome area, called amassif, is relatively new. Because of this, the Adirondacks have been referred to as "new mountains from old rocks." It is theorized that there is a "hotspot" beneath the region, which causes continued uplift at the rate of 1.5-3 cm annually.[6][7]
TheAppalachian Plateau is a large, dissected plateau region in the eastern United States. It extends from New York southwest to Alabama. It runs parallel to Lake Erie on the northwest, but does not include the land adjacent to the Great Lakes. The plateau is composed of sedimentary rocks, including sandstones, conglomerates, and shales, that were deposited during the latePaleozoic Era. These rocks are generally flat-lying, but have been dissected by streams to form a rugged and mountainous terrain. In addition to these sedimentary rocks, beds of coal are locally significant throughout the Appalachian Plateaus, making this area the heart of the American coal industry.[8]
The Appalachian Plateau includes several physiographic sections:
TheBlue Ridge province is a physiographic province of the larger Appalachian Highlands physiographic division.[9] This province is about 580 miles long and consists of northern and southern physiographic sections, which divides near the Roanoke River gap.
The northern section runs along a narrow ridge from just south ofHarrisburg, Pennsylvania.
The southern section is a plateau area that stretches to northern Georgia, with the southernmost point nearAmicalola Mountain in Dawsonville, Georgia with the westernmost section being nearCohutta Mountain inMurray County, Georgia. The Blue Ridge Mountains are named for their distinctive blue haze, which is caused by the presence of atmospheric pollutants and water vapor.[10] This contributes to the characteristic haze on the mountains and their perceived color.[11]
The mountains are made of highly deformed metamorphic rocks, largely developed during the Precambrian age over 541 million years ago. The mountains include schists, gneisses, slates, and quartzites, and are extensively intruded by igneous bodies. The Blue Ridge Mountains contain the highest mountains in eastern North America south ofBaffin Island. The highest peak in the Blue Ridge isMt. Mitchell in North Carolina at 6,684 feet.[12]
The Piedmont province is a physiographic province of the larger Appalachian Mountains range. It is located in theeastern United States and stretches about 900 miles from New York to Alabama. The province starts inRockland County, New York nearSouth Mountain on the west side of theHudson River.[13]
The eastern border of the Piedmont runs along afall line, the point at which rivers traditionally drop rapidly from harder metamorphic rocks to softer sedimentary rocks.[14] Because the fall line is the spot where rivers become unnavigable, port cities typically have sprung up where rivers cross this boundary. The east side of the Piedmont runs along the Hudson, parallel toManhattan, New York City, throughNew Jersey, and then along a line nearPhiladelphia,Baltimore,Washington, D.C.,Richmond, Virginia,Raleigh, North Carolina,Columbia, South Carolina,Augusta, Georgia,Macon, Georgia, andMontgomery, Alabama. Richmond and Raleigh are both located within the boundaries of the Piedmont. The west side of the Piedmont runs through lesser populated areas, from south of Harrisburg toLake Martin inElmore County, Alabama.[15]
There are two sections of the Piedmont. The primary portion is called the Uplands section. There are two unconnected sections of the province, known as the lowlands, in the New York City and Harrisburg, Pennsylvania areas.
The Piedmont is characterized by rolling hills and valleys that are underlain by crystalline metamorphic rocks. The Piedmont is a region of great geological diversity. It is underlain by a variety of rocks that range in age from Precambrian to Cenozoic. The oldest rocks in the Piedmont are gneisses and schists that formed more than a billion years ago during the Grenville orogeny. These rocks were later intruded by granites and other igneous rocks during the Paleozoic era. During the Mesozoic era, the Piedmont was covered by shallow seas that deposited layers of sandstone, shale, and limestone. These sedimentary rocks were later deformed and uplifted during the Cenozoic era.[16]
The Piedmont is also home to several important mineral resources. The region has long been known for its deposits of gold, which were mined extensively during the 19th century. Other important minerals found in the Piedmont include copper, iron, mica, and granite.[17]
The New England province is a physiographic province of the larger Appalachian Highlands division of the United States. It includes five subdivisions: the New England Uplands, New England Seaboard Lowland, Green Mountain, White Mountain, and Taconic.[18]
Much of the New England province’s bedrock aquifers are in consolidated rocks of sedimentary, igneous, and metamorphic origin. Some of these aquifers, mainly in the western portion of Vermont, consist of carbonate rocks (primarily limestone, dolomite, and marble). These consolidated rocks yield water primarily from bedding planes, fractures, joints, and faults, rather than from intergranular pores.[19]
Like the adjacent physiographic provinces, a large part of the New England province was peneplained during the Jurassic and Cretaceous periods, then uplifted, extensively dissected, and finally glaciated.[20]
The St. Lawrence Valley is a physiographic province of the larger Appalachian division, containing only the Champlain physiographic section.[21] The St. Lawrence Plain is a vast, flat plain, with elevations rarely exceeding 300m (1,000 feet) in Vermont and New York. This area was originally a forest-wetland complex, although very little of the forest remains today.[22]
The province abuts the eastern edge of the St. Lawrence River in New York along the Canadian border and contains most of Lake Champlain in Vermont and New York. Most of the northern border of the St. Lawrence Valley province is adjacent to a physiographic division in Canada that is not part of the Appalachian Mountains in that country. Canada considers all land of the St. Lawrence Valley to be part of the Central Lowlands. The part of the St. Lawrence Valley province that abuts the Appalachian Uplands of Canada meets the Eastern Quebec Uplands.[23]
TheValley and Ridge province is a physiographic province of the larger Appalachian division, located in the eastern United States. It is bordered on the east by the Blue Ridge and Piedmont provinces and on the west by the Appalachian Plateau. There are three sections of the province, the Hudson section, the Central section, and the Tennessee section.[24]
The province is a series of northeast-southwest trending synclines and anticlines composed of early Paleozoic sedimentary rocks. Limestones and shales are more susceptible to erosion and make up much of the valleys, whereas more resistant sandstones and conglomerates form the ridges.[25]
The Valley and Ridge province extends for nearly 1,200 miles (1,930 km) from the St. Lawrence Valley in upstate New York to the Coastal Plain of central Alabama. Its width varies from 14 to 80 miles (23 to 130 km). The area is home to many valuable resources, both economic and geo-heritage. Vast beds ofanthracite coal exist in Pennsylvania and are mined at depths up to 600 m (2,000 ft). Iron and Zinc are also produced in the Valley and Ridge province, mined from the minerals hematite (iron) and sphalerite (zinc).[26]
blue mountains chemical terpene.
